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Record W7084189930

Geochemistry Implications of Runoff at the Livestock and Forage Centre of Excellence

2025· article· en· W7084189930 on OpenAlexfundno aff

Bibliographic record

VenueUniversity Library (University of Saskatchewan) · 2025
Typearticle
Languageen
FieldMedicine
TopicSepsis Diagnosis and Treatment
Canadian institutionsnot available
FundersGlobal Water Futures
KeywordsSurface runoffFeedlotHydrology (agriculture)LivestockForageGroundwaterRainwater harvestingRunoff curve number
DOInot available

Abstract

fetched live from OpenAlex

The objectives of this research were to determine the potential volume losses of water and associated constituent ions contained in cattle feedlot runoff through the runoff ditches at the USask Livestock and Forage Center of Excellence and the fate of the major anions and cations typically found in cattle feedlot runoff as they transport through the subsurface soils. This was accomplished through the investigation of the transport of five major cations (Ca2+, Mg2+, K+, Na+, and NH4+) and three major anions (Cl-, HCO3-, and SO42-) in laboratory soil columns. The columns were packed with two different soils: a clay present in the pen floors, and a silty clay present in the drainage ditches. The columns were then equilibrated with groundwater from the site. A simulated feedlot runoff solution was then flushed through the soil columns, followed by a simulated rainwater solution to represent season impacts. The breakthrough curves obtained by both stages of the experiment were used to identify key processes affecting the transport of the species. During the simulated runoff stage, Ca2+ was replaced on the exchange sites by Na+, K+, and NH4+ for all the columns (both soils). Generally, ions with higher valency will exchange for those of lower valency, but the majority of the ions in the feedlot runoff solution have a lower valency, replacing those of higher valency, such as Ca2+, through mass action. Ca2+ was replaced first, followed by Mg2+ once the ionic strength of the solution was higher. All columns had HCO3- concentrations below input concentrations. This was believed to be due to the precipitation of carbonate minerals. The pen clay columns demonstrated SO42- concentrations much higher than input concentrations. This, along with the high Ca2+ concentrations in the column effluent suggested that gypsum (CaSO4) dissolution was occurring from the soil. The solubility of gypsum at 25°C is 2000-2500 mg/L (Lebedev and Kosorukov 2017) and the average effluent concentration of SO42- was approximately 1600 mg/L which appeared to confirm the source of sulphate in the effluent. Simulated rainwater was then placed on top of the columns to assess the permanency of the attenuation of ions of interest. In all columns the effluent contained excess K+ and Na+, indicating the previously attenuated ions came back into solution off the exchange complex. There was also excess HCO3- and Ca2+, suggesting the dissolution of calcite. In the ditch silty clay columns, the concentration of Mg2+ was below the input concentration, indicating Mg2+ was sorbed on the exchange complex, replacing Na+, K+, and NH4+. In the pen clay columns, the SO42- and Ca2+ concentrations in the effluent remained well above the input concentrations. This suggests the dissolution of gypsum continued during the rainwater flushing stage.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.234
Threshold uncertainty score0.540

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.012
GPT teacher head0.204
Teacher spread0.191 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

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